South-central Texas · Texas

Edwards Aquifer

Is the Edwards Aquifer running dry?

Edwards Aquifer serves about 2.5 million people and underpins roughly $5B of agriculture across Texas. This model puts its probability of reaching crisis conditions at 53.2% by 2100 (95% CI 52.7%–53.6%), making it the highest-risk system in this analysis. Expected crisis year is approximately 2058. Measured water levels are falling about 0.05 ft/yr.

Key figures

Crisis probability by 204012.2%
Crisis probability by 206032.0%
Crisis probability by 210053.2% (95% CI 52.7%–53.6%)
Expected crisis year2058
Observed decline rate0.0548 ft/yr
Latest observed level99.24 (2025)
Year-to-year volatility19.270
Drought persistence φ (AR(1))0.2641
Population served2.5M
Agricultural value$5B
Modelled annual damage at crisis$2.75B

Monitoring wells in this system

Aquifer averages hide local stress. These are the Edwards wells that appear in the 20 most at-risk sites nationally.

WellStateDecline (ft/yr)P(crisis) 2060Expected crisis
Seco Creek WellTX2.70100.0%2026
Western OakTX2.38100.0%2026
Parkwood ParkTX1.89100.0%2026
Z DEDTX2.42100.0%2026
AY-68-28-516TX1.79100.0%2026
AY-68-28-406TX1.63100.0%2026
JY-65-26-812TX0.8167.8%2045
JY-65-26-520TX0.8090.3%2035

How to read these numbers

Crisis probabilities are modelled, not measured: 100,000 Monte Carlo paths per aquifer combining AR(1) drought persistence with CMIP6 warming and demand-supply coupling. Observed decline rates and water levels are measured from USGS monitoring wells. A low aquifer-average probability does not mean local wells are safe — the well table above frequently disagrees with the system average. Full method on the science page, and every input is traceable through the research index.